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The Somerset Levels have an area of about 160,000 acres (650 km 2) and are bisected by the Polden Hills; the areas to the south are drained by the River Parrett, and the areas to the north by the rivers Axe and Brue. The Mendip Hills separate the Somerset Levels from the North Somerset Levels. The Somerset Levels consist of marine clay "levels ...
Around 70% of deep peat in the Somerset Levels and Moors is likely to be losing carbon due to intensive livestock grazing, cultivation and direct extraction. Maize cultivation has increased, and most soils under maize were damaged to the extent that rainfall is unable to penetrate the upper soil layers, resulting in silt-laden runoff.
The Somerset Levels and surrounding hills. Somerset is a rural county in southwest England with an area of 4,171 square kilometres (1,610 sq mi). It is bounded on the north-west by the Bristol Channel, on the north by Bristol and Gloucestershire, on the east by Wiltshire, on the south-east by Dorset, and on the south west and west by Devon.
North Somerset Levels taken from Dolebury Warren. The North Somerset Levels is a coastal plain, an expanse of low-lying flat ground, which occupies an area between Weston-super-Mare and Bristol in North Somerset, England. The River Banwell, River Kenn, River Yeo and Land Yeo are the three principal rivers draining the area.
Bearley Brook; Black Ditch; Cannington Brook; Chinnock Water; Cobb's Cross Stream; Decoy Rhine; Eighteen Foot Rhine; Hamp Brook; Horsey Pill; King's Sedgemoor Drain
Large areas of peat were laid down on the Somerset Levels, particularly in the River Brue Valley, during the Quaternary period after the ice sheets melted. [10] The extraction of peat from the Moors is known to have taken place during Roman times, and has been carried out since the Levels were first drained. Peat extraction on the Somerset ...
This category groups together articles relating to the Somerset Levels, England. Pages in category "Somerset Levels" The following 100 pages are in this category, out of 100 total.
The floods were the worst in local memory. A study commissioned by the Environment Agency from hydraulics consulting firm HR Wallingford concluded that it was among the most extreme ever experienced in Britain. The peak flow was about 140 m 3 /s, between 5:00 pm and 6:00 pm BST.